852
find out thermal-land-cover-types was attempted. The
data used for clustering were the temperature-value-
frequency-histcgrams (30 one-degree temperature vari
ables) of the micropixels being united in the macro
pixels of 25x25, 50x50 and 100x100 pixels size. As
input for the clustering algorithm only the number n
of the desired clusters has to be specified and in an
iterative process all the macropixels were classified
to the nearest of the n cluster centers. As distance
measure the Euclidian distance was used. The best
interpretable results were obtained by choosing six
cluster centers. The cluster-macropixels were plotted
in the same manner as the temperature-macropixels
and Fig.3 to Fig.6 show the results.
In the 100 x 100 macropixelfield only the dense
woodland (cluster 6), large fields with maize (clus
ter 5) and harvested fields or asphalted areas (clus
ter 4) can be identified quite well. The rest are more
or less mixed areas and not clearly interpretable.
In the 50 x 50 macropixelfield (Fig. 4) the clusters
can be interpreted in the following way:
Cluster 1: fields cultivated with maize, single-fami
ly-houses with large vegetated areas around.
Cluster 2: single-family-houses , small regular struc
ture, quarters with modern house-blocks and large
vegetated areas in between.
Cluster 3: green fields or meadows.
Cluster 4: bare soil areas, harvested fields, industri
al areas, railway and other traffic areas, motorway.
Cluster 5: mixed areas with high rate of vegetation.
Cluster 6: wood, large parks, water.
In Fig. 6 the 25 x 25 macropixelfield possesses the
following clusters:
Cluster 1: centers of large green fields, meadows,
mixed fields.
Cluster 2: single-family-houses with regular structure.
Cluster 3: green fields, edges of fields, meadows,
clearings.
Cluster 4: inner city without vegetation, harvested
fields, motorway, house-blocks with warm roofs,
railway areas.
Cluster 5: harvested fields, industrial areas, rail
way areas, sports-grounds.
Cluster 6: wood, house-blocks with large shadows,
partly gardens and tree groups.
When we compare Fig.4 and 5 where only five clusters
were determined we can see the mixture in cluster
ordination (see table 6).
6 CONCLUSION
It is not possible to classify thermal images into
very special land use classes like we can do with
multispectral data because most of the land use clasj
which can be separated very well in visible and near
infrared light have overlapping sinature intervalls
in one dimensional thermal infrared data. This can be
seen very clearly from a table where different land
cover classes and their thermal signature are listed
(see Seger & Mandl 1985, p.73).
So only thermal more or less homogenious classes or
urban cover types can be separated. This separation
can be done for instance by image enhancement methods
namely generalization in the radiometric and/or spa
tial domain or unsupervised classification using
clustering of simple texture parameters like the
temperature-value-histogram parameters in our study.
The extracted classes should only be characterized
in a qualitative way and a correlation with a ground
truth map showing conventinal land use classes will
only bring good results when the classes have very
rough definition.
We have to choose a certain level of generalization
in all domains (spatial, radiometric and temporal)
and choose corresponding methods to answer the questio:
of the special work.
REFERENCES
Lee, D.O. 1984. Urban climates. Progress in Physical
Geography 8:1-31.
Nübler, W. 1979. Konfiguration und Genese der Wärme
insel der Stadt Freiburg. Freiburger Geographische
Hefte, Heft 16. Freiburg i. Br.
Oke, T.R. & F.G.Hanneil 1970. The form of the urban
heat island in Hamilton, Canada. In WMO, Urban
Climates. Technical Note No.108. Geneva.
Seger, M. & P.Mandl 1985. Strahlungstemperaturbilder
als Beitrag zur Stadtklimatologie. In M.Seger (ed.) (
Forschungen zur Umweltsituation in Klagenfurt,
p.59-93. Klagenfurt.
Table 6. Crosstable representing the number of macro
pixels classified in the clusters of Fig. 4 and 5.
Clusters
Fig. 4
Clusters
1 2
Fig. 5
3
4
5
sum
1
45
388
2
16
29
480
2
O
185
8
7
0
200
3
44
0
0
0
0
44
4
0
0
1
116
1
118
5
0
0
13
0
0
13
6
0
0
0
0
153
153
sum
89
573
24
139
183
1008
When we do the same comparision using figures 3, 4
and 6 no trend is discernible. We can see this fact
also in the different descriptions of the clusters
from Fig. 3, 4 and 6. That means that the different
levels of spatial generalization represented by the
different macropixelsize are more important for an
urban-land-cover-type adequate classification of the
thermal infrared image than the actual number of
clusters in a certain range. For this reason the veri
fication of the cluster-images (figures 3 to 6) were
only done qualitatively and not quantitatively by
correlating the maps with a handdrawn ground truth
land use map.
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